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Hydraulic Conductivity Estimation Test Impact on Long-Term Acceptance Rate and Soil Absorption System Design

机译:水力传导率估算测试对长期接受率和土壤吸收系统设计的影响

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The aim of this paper was to verify the common methods of hydraulic conductivity estimation for soil assessment in respect to wastewater disposal. The studies were conducted on three types of sandy soils. Hydraulic conductivity was determined using a scale effect-free laboratory method, empirical equations and compared with measurements estimated from a laboratory infiltration column with identified head loss. Based on the hydraulic conductivity values, the long-term acceptance rates (LTAR) [1] were calculated. The differences in LTAR values were about one order of magnitude smaller than differences in hydraulic coefficient. The study showed a good convergention of the results obtained from the constant head method (CHM) by solving the Glover Equation for medium and coarse sands. In low permeability soil (fine sand), the best result was obtained using CHM-a with a capillary rise consideration (a is a factor included in the flow in the unsaturated and saturated zones calculated from a capillary rise). From a practical point of view the relatively small value of LTAR underestimation (20%-for constant head method) is responsible for the extended surface area of the system and provides a security margin (the avoidance of clogging risk). The use of the falling head method, based on the Van Hoorn equation, can be said to be highly overestimated. For medium and coarse sandy soils the underestimation of LTAR calculated and based on CHM test determination is 14%–18%. The total cost of soil absorption system (SAS) designed-based on CHM in comparison to that designed-based on real hydraulic conductivity value in Poland is only about 7%–9% higher.
机译:本文的目的是验证有关废水处理的土壤评估中水力传导率估算的常用方法。研究是在三种类型的沙质土壤上进行的。使用无垢效应的实验室方法,经验方程式确定水力传导率,并与从实验室渗透柱估计的水头损失估计值进行比较。根据水力传导率值,计算出长期接受率(LTAR)[1]。 LTAR值的差异比水力系数的差异小约一个数量级。研究表明,通过求解中,粗砂的Glover方程,可以很好地融合恒头法(CHM)的结果。在低渗透性土壤(细砂)中,使用考虑了毛细管上升的CHM-a可获得最佳结果(a是从毛细管上升计算得出的非饱和和饱和区域中的流动因子)。从实际的角度来看,LTAR的相对较低的值被低估了(对于恒定压头方法,为20%)导致了系统表面积的扩大,并提供了安全裕度(避免了堵塞风险)。基于Van Hoorn方程的落头法的使用可以说被高估了。对于中,粗砂质土壤,根据CHM测试确定计算得出的LTAR低估为14%–18%。在波兰,基于CHM设计的土壤吸收系统(SAS)的总成本与基于真实水力传导率设计的土壤吸收系统的总成本相比仅高7%–9%。

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